Climatic induced snowpack surfaces on Lebanon's mountains.

A. Shaban, T. Darwich, L. Drapeau, S. Gascoin
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引用次数: 5

Abstract

There are tremendous aspects of water resources in Lebanon where the surface water sources are the most ex- ploited. However, snow is still the major water aspect that plays a role in feeding groundwater, springs and rivers. This water resource has been ignored since long-time and it was considered only for tourism. Nevertheless, the recently existed challenges on water supply in the region, notably the challenging climatic variability, makes it necessary to monitor the behavior and dynamics of snowpack on the mountainous regions of Lebanon. Therefore, several studies have been carried out in this respect, focusing on the use of space observations along several time series. While, few concerns were given to the physical characteristic and behavior of snow melt that resulting water flow regime. This study includes two major components of investigation. These are: the analysis of remotely sensed data to monitor snow cover area and the direct in- vestigation of snow samples in the field to measure the melting rate and patterns. Therefore, daily MODIS satellite im- ages, with moderate spatial resolution, were analyzed to detect any changing in the snow cover area, as well as to deduce the accumulation and melting regime. Whereas, field investigations were applied to 275 sites with different altitudes, dates and terrain aspects. The measures were analyzed to identify the relationship between snow cover dynamic, snow materials characteristics and the physical setting. Thiswill be a helpful tool to identify the climate control on the snow- pack; in addition, it contributes for new inputs on water resource management approaches, notably in the view of chang- ing climatic regime.
黎巴嫩山区的气候导致积雪表面。
黎巴嫩的水资源有许多方面,其中地表水资源被开发得最多。然而,雪仍然是水的主要方面,在补给地下水、泉水和河流中起着重要作用。长期以来,这种水资源一直被忽视,只被认为是旅游资源。然而,该区域最近存在的供水挑战,特别是具有挑战性的气候变化,使得有必要监测黎巴嫩山区积雪的行为和动态。因此,在这方面进行了若干研究,重点是利用沿若干时间序列的空间观测。然而,很少有人关注雪融化的物理特性和行为,从而导致水流状态。本研究包括两个主要组成部分的调查。这两种方法分别是:利用遥感数据分析积雪覆盖面积;实地直接调查积雪样品,测量积雪融化速度和模式。因此,我们分析了中等空间分辨率的MODIS卫星日图像,以检测积雪面积的变化,并推断积雪的积累和融化情况。对275个不同海拔、不同日期和不同地形的地点进行了实地调查。分析了积雪动态、积雪材料特征与物理环境之间的关系。这将是一个有用的工具,以确定气候控制积雪;此外,它还有助于在水资源管理方法方面,特别是在气候变化方面,提供新的投入。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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